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• 31. Supporting structures stopped most of an avalanche

  A snow avalanche was released from the Tvísteinahlíð mountain by the health care centre at Engihlíð in Ólafsvík on 19 March 2012. The fracture line of the avalanche was near the top of the slope and extended from the gully to the west of the hillside and into supporting structures that have been installed as protection measures to reduce avalanche danger in the settlement /avalanches/articles/nr/2475

• 32. Vertical displacement in the Bárðarbunga caldera

  September 2014. The gray line represents relative displacement and the blue line the median value for 180 minutes. Earthquakes in the area are shown separately below (same x-axis, same timing). Enlarge. The first two weeks as an example Total subsidence from 12 Sept 2014 until 1 March 2015 The total subsidence of the glacier surface above the Bárðarbunga caldera since the equipment /earthquakes-and-volcanism/gps-measurements/bardarbunga/caldera

• 33. Supporting structures stopped most of an avalanche

  of a town in north Iceland in 2012 27.4.2012 A snow avalanche was released from the Tvísteinahlíð mountain by the health care centre at Engihlíð in Ólafsvík on 19 March 2012. The fracture line of the avalanche was near the top of the slope and extended from the gully /about-imo/news/nr/2476/

• 34. Supporting structures stopped most of an avalanche

  in north Iceland in 2012 Tómas Jóhannesson 25.4.2012 A snow avalanche was released from the Tvísteinahlíð mountain by the health care centre at Engihlíð in Ólafsvík on 19 March 2012. The fracture line of the avalanche was near the top of the slope and extended from /avalanches/articles/nr/2475/

• 35. 2013_001_Nawri_et_al

  atlas files follows the standard developed by Risø National Laboratory (Troen and Petersen, 1989). An anno- tated example is shown in Figure 3. The header line contains information about the model run, the index numbers of the particular grid point, the local surface roughness length (SRL), as well as a triplet of numbers with longitude in degrees east, latitude in degrees north, and height above /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 36. Significant ground

  (in the satellite's line-of-sight) associated with the magnitude 5.6 earthquake. Additional deformation is observed in the vicinity of Driffell and east of Keilir, related to movement on faults in this region. Multiple fractures, related to these earthquakes, have been observed on the ground in this area.These earthquakes are related to the volcano-tectonic reactivation of the Reykjanes Peninsula which /about-imo/news/satellite-images-show-significant-ground-deformation-associated-with-earthquake

• 37. Status of unrest in Reykjanes

  August 2022 showing new dike intrusion on Reykjanes Peninsula and deformation associated with the M5.47 earthquake on 31 July 2022. Coloured fringes show ground deformation in the satellite's line-of-sight, related to the new dike intrusion beneath Fagradalsfjall which commenced on the 30th July 2022. The interferogram shows approximately 16 cm of northwestward displacement related /about-imo/news/status-of-unrest-in-reykjanes

• 38. Eruption has started in Grímsvötn

  at Keflavik International Airport, at 220 km distance from the volcano. The cloud extends above a large part of Vatnajökull ice cap. The line marks the approximate location of Grímsvötn volcano. The last eruption in Grímsvötn occurred in November 2004. Grímsvötn is Iceland's most frequently erupting volcano. The figure below shows tremor activity in Grímsvötn associated with the eruption. Note /about-imo/news/nr/2174

• 39. Articles

  (dyn) 23rd and 24th August. The amplitude is shown in three frequency bands (0,5-1 Hz; 1-2 Hz; 2-4 Hz). A low frequency tremor pulse (red line) is clearly seen just before noon 23rd August. Of interest - Bárðarbunga Reduction of the accesscontrolled area around Holuhraun lava field END /earthquakes-and-volcanism/articles/bigimg/2970

• 40. norsem_asdis

  of Eyjafjallajökull, at approximately 5-7 km depth. The high velocity zones are elongated in the east-west direction, in line with geological surface features and are separated by a zone of relatively lower velocity (3.0 km/s), where earthquakes prior to and during the 2010 summit eruption were located. The high velocity zones most likely correspond to intrusive bodies similar to those previously imaged /media/norsem/norsem_asdis.pdf